沉积与特提斯地质Issue(4)：95-99,5.
重庆吴家湾铝土矿矿床地质特征及控矿因素探讨
Geology and controls of the Wujiawan bauxite deposit in Nanchuan, Chongqing
摘要
Abstract
The ore-bearing rock series of the Wujiawan bauxite deposit in Nanchuan, Chongqing are overlain by the Middle Permian Liangshan Formation ( P2 l ) , and disconformably upon the silty shales of the Middle Silurian Hanjiadian Formation or the limestones of the Middle Carboniferous Huanglong Formation. This bauxite deposit is characterized by high SiO2 , high S, high Fe and low grades of bauxite ores. The bauxite orebodies are in general agreement in occurrence modes with the associated strata, and the ores occur as the earthy, pisolitic (oolitic), densely massive and gravelly forms. The ore-controlling factors of the bauxite deposit include palaeoenvironmental, palaeogeomorphological, structural and stratigraphic factors. The results of research in this study may be helpful for the exploitation and utilization of the bauxite deposits in Wujiawan and throughout southern Chongqing.关键词
铝土矿/地质特征/控矿因素/吴家湾/重庆Key words
bauxite/geology/ore-controlling factor/Wujiawan/Chongqing分类
天文与地球科学引用本文复制引用
凌小明,赵晓东,李军敏,陈莉,吕涛..重庆吴家湾铝土矿矿床地质特征及控矿因素探讨[J].沉积与特提斯地质,2013,(4):95-99,5.基金项目
中国地质调查局渝东地区地质构造演化及铁铝基地研究(1212011085167) （1212011085167）
